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Praehexasaturnalis merici Tekin 2002
No full text<p> <i>Praehexasaturnalis merici</i> Tekin, 2002 (Fig. 10F, G)</p> <p> <i>Praehexasaturnalis merici</i> Tekin, 2002a: 185, pl. 2, fig. 7-9.</p> <p>OCCURRENCE. — Lower Jurassic, uppermost Hettangian-upper Pliensbachian of Antalya Nappes, NE of Antalya city and Mersin Mélange, NW of Mersin city, southern Turkey.</p>Published as part of <i>Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, pp. 493-537 in Geodiversitas 42 (27)</i> on page 518, DOI: 10.5252/geodiversitas2020v42a27, <a href="http://zenodo.org/record/4447758">http://zenodo.org/record/4447758</a>
Praeudalia Tekin 2020, n. gen.
No full textGenus Praeudalia Tekin, n. gen. urn:lsid:zoobank.org:act: 7F321497-E109-4829-94BB-64E5ABB41432 TYPE SPECIES. — Praeudalia rhaetica Tekin, n. gen., n. sp. ETYMOLOGY. — For the occurrence precedent to Udalia Whalen & Carter, 1998. OCCURRENCE. — Late Triassic, Rhaetian of Queen Charlotte Islands, British Columbia, Canada; El Castillo Mélange, Nicaragua / Costa Rica Border; NE of Antalya city and Mersin Mélange, NW of Mersin city, southern Turkey. INCLUDED TAXA. — Praeudalia rhaetica Tekin, n. gen., n. sp., Spumellaria gen. and sp. indet. A (sensu Tekin 2002b). DESCRIPTION Cortical shell includes Pseudoaulophacid structure composed of meshwork of equilateral, triangular pore frames with rounded nodes at vertices. Four spines about similar in length, wide at the base and tapering distally, with sharp ends. Spines coplanar and tetracarinate with very wide grooves adjacent to very narrow ridges. REMARKS This genus differs from Udalia (in Carter et al. 1998: 59) by having tetracarinate instead of tricarinate spines. Praeudalia rhaetica Tekin, n. gen., n. sp. (Fig. 7 A-D) urn:lsid:zoobank.org:act: 018D810C-5979-4B09-AE11-9E56620CF889 Spumellaria gen. and sp. indet. B – Carter 1993: 92, pl. 13, figs 6, 8, 11. — Baumgartner et al. 2008: pl. 3, fig. 11. Spumellaria gen. and sp. indet. A – Tekin 1999: 124, pl. 23, fig. 7. HOLOTYPE. — Sample Orbuk-15, HU.JMB.0114 (Fig. 7A). PARATYPES. — HU.JMB.0115 (Fig. 7B), HU.JMB.0116 (Fig. 7C), HU.JMB.0117 (Fig. 7D). TYPE LOCALITY. — Orbuklukeli section Mersin Mélange, NW of Mersin city, southern Turkey. ETYMOLOGY. — Because of its occurrence in Rhaetian strata. OCCURRENCE. — Upper Triassic, Rhaetian of Queen Charlotte Islands, British Columbia, Canada; El Castillo Mélange, Nicaragua / Costa Rica Border; Antalya Nappes, NE of Antalya city and Mersin Mélange, NW of Mersin city, southern Turkey. DIMENSIONS (based on four specimens, in µm). — Maximum diameter of the cortical shell: 88-110 (holotype: 100, average: 98.5); Length of longest spine: 70-78 (holotype: 70, average: 74.3). DESCRIPTION Same as of the genus. Cortical shell disc-shaped, large, wider than the length of four spines. REMARKS Same as for the genus. This species differs from another species of Praeudalia Tekin, n. gen., illustrated as Gen. et sp. indet. in Tekin (2002b: 428, pl. 3, fig. 12) by possessing a smaller cortical shell and longer primary spines.Published as part of Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, pp. 493-537 in Geodiversitas 42 (27) on pages 508-509, DOI: 10.5252/geodiversitas2020v42a27, http://zenodo.org/record/444775
Replication data for: [Public Health Policy At Scale: Impact of a Government-sponsored Information Campaign on Infant Mortality in Denmark]
No full textDocumentation file for do-files and datasets corresponding to paper titled:
“Public Health Policy at Scale: Impact of a Government-sponsored Information Campaign on Infant Mortality in Denmark”
Onur Altindag, Jane Greve, and Erdal Tekin
This document describes the datasets, STATA and R programs that replicate the results for the paper “Public Health Policy at Scale: Impact of Government-sponsored Information Campaign on Infant Mortality in Denmark” by Onur Altindag, Jane Greve, and Erdal Tekin, Review of Economics and Statistics, the version that is accepted on February 2021
Replication data for: [Public Health Policy At Scale: Impact of a Government-sponsored Information Campaign on Infant Mortality in Denmark]
No full textDocumentation file for do-files and datasets corresponding to paper titled:
“Public Health Policy at Scale: Impact of a Government-sponsored Information Campaign on Infant Mortality in Denmark”
Onur Altindag, Jane Greve, and Erdal Tekin
This document describes the datasets, STATA and R programs that replicate the results for the paper “Public Health Policy at Scale: Impact of Government-sponsored Information Campaign on Infant Mortality in Denmark” by Onur Altindag, Jane Greve, and Erdal Tekin, Review of Economics and Statistics, the version that is accepted on February 2021
Laxtorum obscurum Tekin 2020, n. sp.
No full textLaxtorum obscurum Tekin, n. sp. (Fig. 12K, L) urn:lsid:zoobank.org:act: C977E9D3-0777-4F5E-9E55-1DB51E89B925 Laxtorum sp. A – Tekin 2002a: 194, 196, pl. 5, fig. 15. HOLOTYPE. — Sample Orbuk-27, HU.JMB.0162 (Fig. 12K). PARATYPE. — HU.JMB.0163 (Fig. 12L). TYPE LOCALITY. — Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. ETYMOLOGY. — From the Latin obscurum, obscure, indistinct, due to its obscure inner structure of test. OCCURRENCE. — Lower Jurassic, lower Sinemurian of Antalya Nappes, NE of Antalya City and Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. DIMENSIONS (based on two specimens, in µm). — Length of horn: 65-70 (holotype: 70, average: 67.5); Maximum length of test: 150- 160 (holotype: 150, average: 155); Maximum width of test: 90-100 (holotype: 90, average: 95). DESCRIPTION Test long, increasing in width gradually to the distal end, conical with four to five post-abdominal segments. Cephalis hemisphaerical with stout, needle-like and pointed apical horn. Thorax and rest of segments subtrapezoidal in outline. Strictures invisible at the surface of test. Surface of the test covered with thick silica layers. Cephalis and thorax with very rare pores, abdomen and the rest of test with large, subcircular to ellipsoidal pores and very rough surface. REMARKS This species has been compared to Laxtorum breve Tekin, n. sp. under the latter taxon. It can be differentiated from Laxtorum hemingense Whalen & Carter in Carter et al. (1998: 80, pl. 25, figs 6-8, 13, 14, 24, 25; pl. 27, figs 5, 6, 16, 20) by having a test with a stout horn and indistinct circumferential ridges.Published as part of Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, pp. 493-537 in Geodiversitas 42 (27) on page 525, DOI: 10.5252/geodiversitas2020v42a27, http://zenodo.org/record/444775
İsmail Tekin ve Metin Bora ile sözlü tarih görüşmesi
No full textBu görüşme Rahime Demir tarafından Yaşayanların Dilinden Kartal başlığı altında gerçekleştirilmiştir. Bu kapsamda yapılan görüşmelerin sayısı 46'dır.1945 yılında İstanbul ilinin Kartal ilçesinde doğan İsmail Tekin, ilçede bahçe işlerinin yaygın olduğunu ve bu geleneğin Ermenilerden devralındığını ifade eder. Ortaokulu bitirdikten sonra iş hayatına atılır ve elektrik işine girer. Çocukluğunda ilçede yaşayan Ermenilerle kurdukları ilişkilere değinir, herhangi bir ayrımcılığın yapılmadığını, kendisinin Ermeni arkadaşları babasının ise Ermeni bir ortağı olduğunu belirtir. 1944 yılında İstanbul ilinin Kartal ilçesinde doğan Metin Bora da Ermenilerle ve Rumlarla çok güzel ilişkiler kurduklarını ve birbirlerine saygı gösterdiklerini ifade eder. Arnavut Ali adıyla bilinen dedesinin çetecilik yapan Rumlara karşı koymak üzere bir çete kurduğunu ve Kuvayı Milliye’nin öncüleri arasında bulunduğunu söyleyen Bora, büyüklerinden bu konuyla ilgili olarak duyduğu hadiseleri de aktarmaktadır.Rahime Demi
Laxtorum breve Tekin 2020, n. sp.
No full textLaxtorum breve Tekin, n. sp. (Fig. 12 D-J) urn:lsid:zoobank.org:act: AAC22989-AF44-439E-8E99-6493848E6229 Laxtorum sp. – Aita & Spörli 1992: pl. 5, fig. 12. HOLOTYPE. — Sample Orbuk-32, HU.JMB.0157 (Fig. 12D). PARATYPES. — HU.JMB.0158 (Fig. 12G), HU.JMB159 (Fig. 12H), JMB.0160 (Fig. 12I), HU.JMB161 (Fig. 12J). TYPE LOCALITY. — Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. ETYMOLOGY. — From the Latin brevis-e – short, brief, due its short shell. OCCURRENCE. — Lower Jurassic, lower Sinemurian of Auckland, New Zealand and Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. DIMENSIONS (based on seven specimens, in µm). — Length of horn: 84-120 (holotype: 100, average: 105.7); Maximum length of test: 132-158 (holotype: 158, average: 141.1); Maximum width of test: 120-168 (holotype: 125, average: 136.1). DESCRIPTION Test short with three post-abdominal segments. Cephalis hemisphaerical with a long horn. Horn needle-like, subcircular in transversal section, slightly decreasing in width distally and terminated in a sharp end. Rest of the test increasing in width very slowly, and decreasing in width at last segment. Collar, lumbar and following strictures not prominent, not visible at the surface of test. Surface of test covered with thick layer of silica with irregular surface. Test bears circular to subcircular pores of different sizes. REMARKS This species differs from Laxtorum hemingense Whalen & Carter in Carter et al. (1998: 80, pl. 25, figs 6-8, 13, 14, 24, 25; pl. 27, figs 5, 6, 16, 20) by having a shorter test with very long horn and indistinct circumferential ridges. It can be differentiated from Laxtorum obscurum Tekin, n. sp. by possessing a thin, long horn and longer test with more segments.Published as part of Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, pp. 493-537 in Geodiversitas 42 (27) on pages 524-525, DOI: 10.5252/geodiversitas2020v42a27, http://zenodo.org/record/444775
Canoptum rarum Tekin 2020, n. sp.
No full textCanoptum rarum Tekin, n. sp. (Fig. 11 V-X) urn:lsid:zoobank.org:act: D8026B8E-0D55-4575-9022-E9AB66091477 HOLOTYPE. — Sample Orbuk-15, HU.JMB.0154 (Fig. 11V). PARATYPES. — HU.JMB.0155 (Fig. 11W), HU.JMB156 (Fig. 11X). TYPE LOCALITY. — Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. ETYMOLOGY. — From the Latin rarum, rare, due to its rare occurrence. OCCURRENCE. — Upper Triassic, Rhaetian, Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. DIMENSIONS (based on three specimens, in µm). — Maximum length of test: 200-220 (holotype: 208, average: 209.3); Maximum width of test: 104-120 (holotype: 104, average: 111.3). DESCRIPTION Test spindle-shaped, multicyrtid with six post-abdominal segments. Test increasing in width gradually up to the third post-abdominal segment, then the last three segments are decreasing in width. Cephalothorax hemisphaerical, mainly poreless. Abdomen to third post-abdominal segment hooplike and strictures between these segments less-prominent, marked only by very shallow depressions. Strictures between third to sixth post-abdominal segments not visible. Because of dense silica accumulation, only small scattered pores are visible on the surface of test. When accumulation of silica is not prominent, two rows of pores can be seen around strictures. On wider part of test, corresponding to the third postabdominal segment, 16 pores are visible in one row. REMARKS This taxon can be differentiated from other species of the genus Canoptum Pessagno by having the spindle-shaped last three segments without superficial strictures.Published as part of Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, pp. 493-537 in Geodiversitas 42 (27) on page 524, DOI: 10.5252/geodiversitas2020v42a27, http://zenodo.org/record/444775
Emiluvia prisca Tekin 2020, n. sp.
No full textEmiluvia prisca Tekin, n. sp. (Fig. 6 W-Y) urn:lsid:zoobank.org:act: 7DE81B35-1355-426F-89AC-1AA538F91A9C HOLOTYPE. — Sample Orbuk-46, HU.JMB.0111 (Fig. 6W). PARATYPES. — HU.JMB.0112 (Fig. 6X), HU.JMB.0113 (Fig. 6Y). TYPE LOCALITY. — Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. ETYMOLOGY. — From the Latin: Prisca: former, ancient, old-fashioned, due to its old occurrence. OCCURRENCE. — Lower Jurassic, middle Lower Pliensbachianupper Pliensbachian, Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. DIMENSIONS (based on three specimens, in µm). — Diameter of test: 92-100 (holotype: 100, average: 97.3); Length of spines: 110- 130 (holotype: 130, average: 118.6). DESCRIPTION Test large, sphaerical to subsphaerical with four spines situated at corners. Very large nodes present at pore frame vertices on the outer layer of cortical shell. Four nodes visible per row. Inner layer of pore frames polygonal (mainly triangular). Spines longer than the diameter of cortical shell and mainly equal, tapering distally, terminated with very sharp end. They are tricarinate with relatively wide ridges and wide grooves. REMARKS This species can be differentiated from Emiluvia tuberis (Carter et al. 1998: 41-42, pl. 5, figs 9, 10, 19) by having a sphaerical to subsphaerical cortical shell with large nodes at pore frame vertices.Published as part of Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, pp. 493-537 in Geodiversitas 42 (27) on page 508, DOI: 10.5252/geodiversitas2020v42a27, http://zenodo.org/record/444775
Canoptum productum Tekin 2020, n. sp.
No full textCanoptum productum Tekin, n. sp. (Fig. 11 R-U) urn:lsid:zoobank.org:act: 4E402E3A-79F5-405C-AB7F-EB5F656496A0 HOLOTYPE. — Sample Orbuk-15, HU.JMB.0150 (Fig. 11R). PARATYPES. — HU.JMB.0151 (Fig. 11S), HU.JMB52 (Fig. 11T), HU.JMB.0153 (Fig. 11U). TYPE LOCALITY. — Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. ETYMOLOGY. — From the Latin productum, lengthened, long, due its long test. OCCURRENCE. — Late Triassic, Rhaetian, Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey. DIMENSIONS (based on four specimens, in µm). — Maximum length of test: 170-220 (holotype: 220, average: 190); Maximum width of test: 80-100 (holotype: 100, average: 89.3). DESCRIPTION Test long, slender, very slowly incerasing in width and height distally with six post-abdominal segments. Cephalothorax dome-shaped, probably without horn, poreless, collar stricture indistinct. Lumbar stricture and other strictures prominent, marked by relatively deep depressions and mainly poreless. Abdomen to post-abdominal segments hoop-like, mainly covered by veneer of thick, microgranular silica with scattered, small, subcircular pores. Two rows of pores (15-16 pores at one row on half a circumference) can be seen just above and below septa located at strictures when silica accumulation is not prominent. REMARKS This species differs from Canoptum merum (Pessagno &Whalen 1982: 124, pl. 1, figs 1, 15, 16, 20; pl. 12, fig. 11) by a having a more slender test covered by prominent silica accumulation, fewer scattered pores and abdomen to last post-abdominal segments hoop-like instead of trapezoidal in outline.Published as part of Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, pp. 493-537 in Geodiversitas 42 (27) on pages 522-524, DOI: 10.5252/geodiversitas2020v42a27, http://zenodo.org/record/444775
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